This paper processes the data of delafossite magnetic anomaly by continuation analysis in a certain region, and it puts forward the related interpretation. The spatial transf can divide the anomaly of geologic body with different depth. It also can furthest prominent magnetic anomaly of the target to better determine the geometry.%本文是用解析延拓的方法对某地区铜铁矿磁异常数据处理,并做了相应的解释。利用场的空间换算就可以划分不同深度的地质体的异常。也可以在目标场源空间深度最大限度地突出目标引起的磁异常,更好地确定其几何形态。
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